| Abstract: | Two outwardly similar shallow‐canyon drainages of the Four Corners region of the Colorado Plateau (southwestern U.S.), McElmo Creek (SW Colorado) and Chaco Wash (NW New Mexico), expose late Holocene units which have been dated by numerous remains of the puebloan Anasazi culture (A.D. 500–1300). The stratigraphic sequences, though composed of similar sediment facies, show markedly different evolutions. The McElmo Canyon sequence consists of two units separated by an unconformity that apparently represents an arroyo that migrated 5 km upstream in 200 years, suggesting a slow “complex response” model. The dated Chaco Canyon sequence includes an arroyo channel fill seemingly cut simultaneously through a 9–14 km reach, which began filling simultaneously throughout about 100 years later. Base level control seems to have been temporarily controlled by a large eolian sand dune damming Chaco Wash, probably during a dry period. The two entrenchment chronologies do overlap, but the resemblance of either record to published regional chronostratigraphies is minimal. The differences among these regional chronologies suggest that great variety existed among fluvial sequences in prehistory, perhaps more than is seen in present‐day drainages of the region. The contrasting fluvial histories correspond to an equally marked difference in cultural responses, especially in water‐control technology. The strongest obvious similarity between the sequences is probable anthropogenic influence, which is a consequence of using cultural remains for establishing chronological control. A strong influence of climate change is less obvious but still probable if lags in the system and possible intraregional paleoclimatic differences are included in the analysis. © 2004 Wiley Periodicals, Inc. |
